Articles | Volume 12, issue 3
The Cryosphere, 12, 907–920, 2018
https://doi.org/10.5194/tc-12-907-2018
The Cryosphere, 12, 907–920, 2018
https://doi.org/10.5194/tc-12-907-2018
Research article
14 Mar 2018
Research article | 14 Mar 2018

Near-surface temperature inversion during summer at Summit, Greenland, and its relation to MODIS-derived surface temperatures

Alden C. Adolph et al.

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Cited articles

Adolph, A., Albert, M., and Hall, D.: Infrared Surface Temperature near Summit, Greenland in June and July of 2015, Arctic Data Center, https://doi.org/10.18739/A2W27K, 2018. 
Ahlstrøm, A. P. and PROMICE project team: A new programme for monitoring the mass loss of the Greenland ice sheet, in: Review of survey activities 2007, edited by: Bennike, O. and Higgins, A. K., GEUS, Copenhagen (Geological Survey of Denmark and Greenland Bulletin 15), 2008. 
ARM Climate Research Facility: Millimeter Wavelength Cloud Radar (MMCRMOM), updated hourly, 1 June 2015–30 July 2018, Summit Station, Greenland (SMT) External Data (satellites and others) (X1), compiled by: Johnson, K. and Bharadwaj, N., Atmospheric Radiation Measurement (ARM) Climate Research Facility Data Archive, Oak Ridge, Tennessee, USA, https://doi.org/10.5439/1025228 (last access: 7 March 2018), 2010. 
Berkelhammer, M., Noone, D. C., Steen-Larsen, H. C., Bailey, A., Cox, C. J., O'Neill, M. S., Schneider, D., Steffen, K., and White, J. W. C.: Surface-atmosphere decoupling limits accumulation at Summit, Greenland, Sci. Adv., 2, e1501704, https://doi.org/10.1126/sciadv.1501704, 2016. 
Box, J. E.: Greenland ice sheet surface mass balance reconstruction. Part II: surface mass balance (1840–2010), J. Climate, 26, 6974–6989, https://doi.org/10.1175/JCLI-D-12-00518.1, 2013. 
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Short summary
In our studies of surface temperature in Greenland, we found that there can be differences between the temperature of the snow surface and the air directly above, depending on wind speed and incoming solar radiation. We also found that temperature measurements of the snow surface from remote sensing instruments may be more accurate than previously thought. Our results are relevant to studies of climate change in the remote sensing community and in studies of the atmospheric boundary layer.